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Goose Creek Watershed Management Plan Version - Charlotte ...

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<strong>Goose</strong> <strong>Creek</strong> <strong>Watershed</strong> <strong>Management</strong> <strong>Plan</strong> <strong>Version</strong> 1...………………...October 31, 2009<br />

Figure 8: Distribution of Land Uses in the <strong>Goose</strong> <strong>Creek</strong> <strong>Watershed</strong>.<br />

2.2.6 Soils<br />

The distribution of soils within the <strong>Goose</strong> <strong>Creek</strong> <strong>Watershed</strong> was determined through the<br />

Soil Survey of Mecklenburg County (USDOA – SCS, 1980). The hydrologic soil types<br />

found in the <strong>Goose</strong> <strong>Creek</strong> <strong>Watershed</strong> are B and C. A description of each soil type and<br />

distribution within the watershed are shown in Table 7. Figure 9 shows the location of<br />

the hydrologic soil groups in the <strong>Goose</strong> <strong>Creek</strong> <strong>Watershed</strong>.<br />

Table 7: Hydrologic Soil Groups Found Within the <strong>Goose</strong> <strong>Creek</strong> <strong>Watershed</strong>.<br />

Hydrologic<br />

Soil Group<br />

MATTHEWS-MINT HILL<br />

DAVID<br />

FOUR OAKS<br />

WELL<br />

IDLEFIELD<br />

MINTWOOD<br />

HOODRIDGE<br />

PEGGY<br />

PIAFFE<br />

BEECH MINT<br />

DAVIS TRACE<br />

BLACKJACK<br />

CRESTHILL<br />

LAWYERS<br />

THOMPSON<br />

YARMOUTH<br />

BAIN SCHOOL<br />

JOLI CHEVAL<br />

MCWHIRTER<br />

FOX HOLLOW<br />

Description (USDOA –SCS, 1980) Distribution with<br />

<strong>Goose</strong> <strong>Creek</strong><br />

B Soils having a moderate infiltration rate when thoroughly wet.<br />

These consist chiefly of moderately deep or deep, moderately<br />

well drained or well drained soils that have moderately fine<br />

texture to moderately coarse texture. These soils have a<br />

JUMPER<br />

moderate rate of water transmission<br />

C Soils having a slow infiltration rate when thoroughly wet.<br />

These consist chiefly of soils that have a layer that impedes the<br />

downward movement of water of soils that have moderately fine<br />

texture or fine texture. These soils have a slow rate of water<br />

transmission.<br />

RANBURNE<br />

KIDWELLY<br />

FAIRVIEW<br />

QUAIL PARK<br />

SILAS ED<br />

I-485<br />

I-485<br />

I-485 INNER<br />

I-485 OUTER<br />

I-485<br />

ALLEN BLACK<br />

14<br />

BRIEF<br />

WHITMIRE<br />

ALEXIS<br />

LONG<br />

FIELDLARK<br />

BRIEF<br />

UNION<br />

BRIEF<br />

FAIRVIEW<br />

PERSIMMON CREEK<br />

BRIEF<br />

HANGING MOSS<br />

BRIEF<br />

QUARTERS<br />

Legend<br />

BRIEF<br />

TARA OAKS<br />

INDIAN TRAIL<br />

existing-landuse-by-catchment<br />

EXISTING LU<br />

GC<br />

TRANS<br />

COMM-H<br />

COMM-L<br />

FRST<br />

GC<br />

HDR<br />

INS<br />

LDR<br />

MDR<br />

MFR<br />

MLDR<br />

OI-H<br />

OI-L<br />

RR<br />

TRANS<br />

VCNT<br />

BRIEF<br />

<strong>Watershed</strong><br />

6314 Acres (88% of<br />

watershed)<br />

856 acres (12% of<br />

watershed)

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